Turbulent Flow In Two and Three DimensionsSource: Bulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 001::page 22Author:Tennekes, H.
DOI: 10.1175/1520-0477(1978)059<0022:TFITAT>2.0.CO;2Publisher: American Meteorological Society
Abstract: Three-dimensional turbulence occurs mainly in convective clouds and in the atmospheric boundary layer. Two-dimensional turbulence is a model for the statistical features of large-scale flows in the atmosphere. The differences between two- and three-dimensional turbulence are discussed, with a minimum of mathematics, in terms of elementary vorticity dynamics. The influence of the microstructure on the evolution of the large-scale features of the flow field is explored in some detail. A simple rationale is given for ignoring subgrid scale fluxes in numerical weather prediction.
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| contributor author | Tennekes, H. | |
| date accessioned | 2017-06-09T14:39:39Z | |
| date available | 2017-06-09T14:39:39Z | |
| date copyright | 1978/01/01 | |
| date issued | 1978 | |
| identifier issn | 0003-0007 | |
| identifier other | ams-23860.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4160468 | |
| description abstract | Three-dimensional turbulence occurs mainly in convective clouds and in the atmospheric boundary layer. Two-dimensional turbulence is a model for the statistical features of large-scale flows in the atmosphere. The differences between two- and three-dimensional turbulence are discussed, with a minimum of mathematics, in terms of elementary vorticity dynamics. The influence of the microstructure on the evolution of the large-scale features of the flow field is explored in some detail. A simple rationale is given for ignoring subgrid scale fluxes in numerical weather prediction. | |
| publisher | American Meteorological Society | |
| title | Turbulent Flow In Two and Three Dimensions | |
| type | Journal Paper | |
| journal volume | 59 | |
| journal issue | 1 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/1520-0477(1978)059<0022:TFITAT>2.0.CO;2 | |
| journal fristpage | 22 | |
| journal lastpage | 28 | |
| tree | Bulletin of the American Meteorological Society:;1978:;volume( 059 ):;issue: 001 | |
| contenttype | Fulltext |